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Attenuation of TNT in seawater microcosms

机译:TNT在海水微观世界中的衰减

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The ability of two differing marine sediments (one clayey, the other sandy) to attenuate the explosive 2,4,6-trinitrotoluene (TNT), dissolved in intertidal seawater from the eastern English coast of the North Sea, was examined using aerobic microcosms. Analysis of the seawater from the microcosms revealed an initial sharp decline in TNT concentration with clayey sediment in both sterilized (to prevent microbial activity) and unsterilized microcosms. This effect did not occur to such a marked extent in similar sterile and non-sterile sandy sediment microcosms and was attributed mainly to sorption of TNT to the fine clay particles of the clayey sediment. As time progressed, the attenuation of TNT in microcosms containing either type of sediment was found to be less in those that had been sterilized compared with those where microbial action proceeded unhindered. Feeding the microcosms, (i.e. supplying extra carbon sources for the microbial communities), appeared to have a small, but perceptible, enhancing effect upon TNT dissipation. The attenuation of TNT was also measured in large microcosms containing 2.5 L of seawater and no sediment. Analysis of the seawater revealed a gradual decline in TNT concentration in non-sterile and fed microcosms compared to their sterile counterpart. Overall, this laboratory study showed that the attenuation of TNT is slow (half-life in seawater ca.1900 days; half-life sand sediment <700 days; half life in clay sediment 130 days) under conditions commonly encountered in coastal waters of the North Sea.
机译:使用好氧性微观世界考察了两种不同的海洋沉积物(一种粘土,另一种沙质)减弱溶解在北海东部英格兰沿海潮间带海水中的爆炸性2,4,6-三硝基甲苯(TNT)的能力。对来自微观世界的海水的分析显示,在灭菌(防止微生物活动)和未灭菌的微观世界中,黏性沉积物的TNT浓度均出现了急剧下降。在类似的无菌和非无菌的沙质沉积物微观世界中,这种作用并未出现如此显着的程度,并且主要归因于TNT对粘土状沉积物细粘土颗粒的吸附。随着时间的流逝,与没有进行微生物作用的那些微生物相比,在经过灭菌处理的那些微生物中,含有任一种沉积物的微观世界中的TNT衰减都较小。喂养微观世界(即为微生物群落提供额外的碳源)似乎对TNT的消散具有很小但可感知的增强作用。在包含2.5 L海水且无沉积物的大型微观世界中,也测量了TNT的衰减。对海水的分析表明,与无菌对虾相比,非无菌和饲喂微生物的TNT浓度逐渐下降。总的来说,该实验室研究表明,在沿海地区通常遇到的条件下,TNT的衰减很慢(在海水中的半衰期约为1900天;在沙子中的半衰期小于700天;在粘土中的半衰期为130天)。北海。

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